Daily Yellowstone journal., 1887-10-14
THE THEORY OF STORMS.
An Easily Understood Description OF
How They Originate and Pass Away.

How They Originate and Pass Away.
Sergt. +. b. Dunn, the signal service
officer in charge Of the station on the
Equitable building, thus explained the
theory Of storms the other DAY:
..Storms are caused" he said. first
by the meeting and commingling Of in
equal atmospheric temperatures or pres
mres; second, by the rotation Of the
earth, and, thirdly, by unequal specific
gravity Of different layers of air. The
first of these causes is the prime one; the
other two are but of secondary and COM
paratiyely slight importance in the gen.
Grafton Of a storm.
at is a well known fact that warm air
rises. 1t is equally well known that the
earth becomes heated by the suns rays
falling upon it, and by the absorption and
radiation Of this stored up heat renders
the temperature higher at the surface
than at elevated points. For a time this
hot air on the surface is kept down by
atmospheric pressure, but there comes a
time when the expansion becomes o
great as to break through the cold air
pressure, and the hot air goes up with a
rush, rising sometimes Ia great height.
As this warm air rises II creates a vacuum
below, and the cooler air PUSHES in from
all sides Ia ill its place. This cool air. as
it gets gradually heated, also rises. and
more cool air PUSHES in to again ill the
vacuum. Right at this point where the
hot air first rises is the center Of a storm.
The vacuum caused by the ascending hot
air sucks into lis vortex the air from
every point Of the compass. and this sue
ton causes wind, but places affected by
q storm thus formed. il will be seen. will
have the wind from different paints Of
the compass. according to their direc-
tion from tie storm center. Thus, a
locality directly south of a storm center
will have the wind from the south, as il
rushes north. When this warm air has
accumulated at a sufficiently high alti-
tude. ami become surrounded by "A cooler
air, the moisture in il begins to condense,
forming rain.
The rushing in # the cool air to fill
the vacuum caused by the rising hot air
gives motion To the accumulation Of
warn Az. and it begins "a whirl about
in a circle. hut al the center all Is calm
and clear. Thus II Is that sometimes we
experience "A u ull in the Storm As il is
called. Such "a brief respite is nothing
more than the passing Of a storm center
directly over head, through which the
sun even may shine unobstuctelly.
AS this storm keeps whirling about
over head IL continues 10 gather energy,
and grows 10y the accession Of more heated
air, exactly us "A SNOWFALL is increased in
diameter by rolling il in the snow. At
Last the accumulation becomes Of such
proportions as To feel the effects of the
eartli's rotation, and it begins to move.
This rotation Of the earth, being from
west to east. gives all the storms of any
extent the same general direction. Such
general direction. however, from west to
east, is liable to reflections from various
causes, such as mountains. conditions Of
the atmosphere, by coming in contact
with other storms or air currents, and
by large areas Of water.
mine out of ten American storms
oilEllliN' III Al' hnfhiittiii'tH i'Ei'iio vi
the northwest. where the warm air Of
the valleys rises aud comes in contact
with the cool air from the great eleva-
tions Of the Rocky mountains. These
storms take a generally southeasterly d.
rection until they get into the dry regions
Of Kansas, and there, becoming fam
ished, A. il were. for want Of moisture,
and as if seeming the water for which
they long from the direction If the great
lake region, they make a turn 10 the
northeast and proceed to the great lakes,
where they absorb abundance If moisture,
and then travel on east, deluging Iii with
this water from the lakes. All such gen
eral storms pass out from this country to
the Atlantic. through the st. Lawrence
valley. Within recent years these Ameri-
can storms have been actually traced
across the Atlantic To Europe, and some
of them even rs far as Asia.
''All storms originate in the same way,
whether on land or at sea: in summer or
IN winter. The undercurrent Of air
which rises need not necessarily he warm
10 make II rise: As, for instance. where
the temperature is below the freezing
point: but the u%ndercurrent must be Of
a higher temperature than that above
and surrounding it 10 force it TO rise. In
other words, a storm is originated by a
commingling Of unequal atmospheric
Temperature. New York Commercial
Advertiser.
En-oa.r.tlxa Ett.h.a-